Complex multi-fault rupture and triggering during the 2023 earthquake doublet in southeastern Türkiye

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Chengli Liu
Thorne Lay
Rongjiang Wang
Tuncay Taymaz
Zujun Xie
Xiong Xiong
Tahir Serkan Irmak
Metin Kahraman
Ceyhun Erman
机构
[1] China University of Geosciences,School of Geophysics and Geomatics
[2] University of California Santa Cruz,Department of Earth and Planetary Sciences
[3] GFZ German Research Centre for Geosciences,Department of Geophysical Engineering, The Faculty of Mines
[4] Istanbul Technical University,Department of Geophysical Engineering
[5] Kocaeli University,Eurasian Institute of Earth Sciences
[6] Istanbul Technical University,undefined
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Two major earthquakes (MW 7.8 and MW 7.7) ruptured left-lateral strike-slip faults of the East Anatolian Fault Zone (EAFZ) on February 6, 2023, causing >59,000 fatalities and ~$119B in damage in southeastern Türkiye and northwestern Syria. Here we derived kinematic rupture models for the two events by inverting extensive seismic and geodetic observations using complex 5-6 segment fault models constrained by satellite observations and relocated aftershocks. The larger event nucleated on a splay fault, and then propagated bilaterally ~350 km along the main EAFZ strand. The rupture speed varied from 2.5-4.5 km/s, and peak slip was ~8.1 m. 9-h later, the second event ruptured ~160 km along the curved northern EAFZ strand, with early bilateral supershear rupture velocity (>4 km/s) followed by a slower rupture speed (~3 km/s). Coulomb Failure stress increase imparted by the first event indicates plausible triggering of the doublet aftershock, along with loading of neighboring faults.
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